

FOLLOWUS
1. Third Institute of Oceanography State Oceanic Administration
2. College of Information Science and Technology Xiamen University
网络首发:2013-09-07,
纸质出版:2013
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Characteristics of nutrients in the Jiulong River and its impact on Xiamen Water, China[J]. 海洋湖沼学报(英文), 2013,31(5):1055-1063.
Chen, B., Ji, W., Chen, J. et al. Characteristics of nutrients in the Jiulong River and its impact on Xiamen Water, China., Chin. J. Ocean. Limnol. 31, 1055–1063 (2013). https://doi.org/10.1007/s00343-013-2263-3
Characteristics of nutrients in the Jiulong River and its impact on Xiamen Water, China[J]. 海洋湖沼学报(英文), 2013,31(5):1055-1063. DOI: 10.1007/s00343-013-2263-3.
Chen, B., Ji, W., Chen, J. et al. Characteristics of nutrients in the Jiulong River and its impact on Xiamen Water, China., Chin. J. Ocean. Limnol. 31, 1055–1063 (2013). https://doi.org/10.1007/s00343-013-2263-3 DOI:
Water samples were collected at 20 sites on 4 occasions in 2009 (twice in May
and once in both August and November) along the Jiulong River
South China to examine how nutrient inputs from the Jiulong River could affect the nutrient status of the Xiamen Water. Samples were analyzed for nitrite (NO2-N)
nitrate (NO3-N)
ammonium (NH4-N)
phosphate (PO4-P)
silicate (SiO3-Si)
salinity
and temperature
to determine the nutrient and trophic status of the river. The results indicate that nutrients are derived mainly from river runoff. NO3-N was the main form of DIN in most parts of the river. In addition
NO3-N
DIN
and SiO3-Si behave conservatively. There is a surplus of DIN and SiO3-Si in the river
and PO4-P is a limitation on phytoplankton growth. The concentration of DIN is typically above 0.60 mg/dm3
and higher than 1.00 mg/dm3 in most parts of the river. The concentration of PO4-P is typically above 0.02 mg/dm3
while the concentration of SiO3-Si is higher than 1.00 mg/dm3. Between 2003 and 2008
samples were collected 3 times per year (May
August and November) at 27 sites in the Xiamen Water and analyzed for NO2-N
NO3-N
NH4-N
PO4-P
salinity
and temperature. We discovered that the Jiulong River was the key source of DIN into the Xiamen Water
but not PO4-P
indicating the reason of the N/P molar ratio imbalance in the Xiamen Water. In the future
the effects of high DIN concentrations on the phytoplankton communities and marine ecosystems of the Xiamen Water shall be studied.
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